Research press release


Scientific Reports

Geoscience: Relationship between two recent New Zealand earthquakes

2010年9月と2011年2月にクライストチャーチ(ニュージーランド)付近で発生した2度の地震の相互関係を調べた研究論文がScientific Reportsに掲載される。この論文では、1回目の地震が、2回目の地震の発生した断層に応力を加えて、破壊に近い状態にすることで、2回目の地震発生の一因となったことが示唆されている。


今回S Stramondoたちは、合成開口レーダーを用いた差分インターフェロメトリィ(DInSAR)技術を用いて、この2つの地震の相互関係を解析した。その結果、2010年9月の地震による破壊で、応力値1バール超の応力が地殻の大きな部分に加わり、それが、2回目の地震発生を引き起こすために十分だったことが判明した。


The relationship between two earthquakes that took place near Christchurch, New Zealand, in September 2010 and February 2011 is examined in a paper published in Scientific Reports. The findings suggest that the first earthquake contributed to the occurrence of the second by loading the fault along which the second event occurred with stress, bringing it closer to failure.

In September 2010, a magnitude-7.1 earthquake occurred in Darfield, about 30 miles west of Christchurch, along the previously unrecognised Greendale fault. A second, magnitude-6.3 earthquake took place near Christchurch city centre in February 2011. According to the Coulomb Stress Triggering theory, once an earthquake occurs, the stress does not dissipate but it propagates in the surrounding area, potentially increasing the occurrence of further earthquakes. But it has remained unclear whether the mainshock of the September 2010 event induced a stress redistribution that triggered the February 2011 event.

Using the Differential Synthetic Aperture Radar Interferometry (DInSAR) technique, Salvatore Stramondo and colleagues analyzed the relationship between the two earthquakes. The results show that the rupture of the September 2010 earthquake loaded a large portion of the crust with stress values exceeding 1 bar, which was sufficient to trigger the second earthquake.

Some seismologists have suggested that the second event may have been the largest of the 4,000 aftershocks recorded over the Greendale fault and the surrounding area between September 2010 and February 2011. Further research is needed to determine whether this is the case or whether the second event is indeed a mainshock that occurred along a second fault, promoted by the stress build-up of the first earthquake.

doi: 10.1038/srep00098


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